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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acp-3-29-2003</doi>
	<article_url>http://www.atmos-chem-phys.net/3/29/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/3/29/2003/acp-3-29-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/3/29/2003/acp-3-29-2003.pdf</fulltext_pdf>
	<start_page>29</start_page>
	<end_page>38</end_page>
	<publication_date>2003-01-28</publication_date>
	<article_title content_type="html">A condensed-mass advection based model for the simulation of liquid polar stratospheric clouds</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>D. Lowe</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. R. MacKenzie</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>N. Nikiforakis</name>
		</author>
		<author numeration="4" affiliations="3">
			<name>J. Kettleborough</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Lancaster University, UK</affiliation>
		<affiliation numeration="2" content_type="html">DAMTP, Cambridge University, UK</affiliation>
		<affiliation numeration="3" content_type="html">Rutherford Appleton Laboratory, UK</affiliation>
	</affiliations>
	<abstract content_type="html">We present a condensed-mass advection based model (MADVEC) designed to
      simulate the condensation/evaporation of liquid polar stratospheric cloud
      (PSC) particles. A (Eulerian-in-radius) discretization scheme is used, making
      the model suitable for use in global or mesoscale chemistry and transport models (CTMs). The mass advection equations are solved using an adaption of
      the weighted average flux (WAF) scheme. We validate the numerical scheme using an analytical solution for multicomponent aerosols. The physics of the
      model are tested using a test case designed by Meilinger et al. (1995). The results
      from this test corroborate the composition gradients across the size distribution under rapid cooling conditions that were reported in earlier
      studies.</abstract>
	<references>
	</references>
</article>

